为了确定施肥类型和施肥时间对中亚热带常绿阔叶林土壤有效氮和pH值的影响,通过在浙江天童木荷林(Schima superba)设置4种施肥处理(对照:不添加;氮添加:100 kg N·hm^-2·a^-1;磷添加:15 kg P·hm^-2·a^-1和氮磷添加100 kg N·hm^-2·a^-1+15 kg P·hm^-2·a^-1),测定了氮磷添加后森林土壤有效氮和pH值的变化。结果表明:1)氮添加显著促进了土壤铵态氮和硝态氮含量的增加,增加幅度随着施氮时间的延长而增加;磷添加对土壤铵态氮含量无显著影响,但能显著降低土壤硝态氮含量;氮磷添加显著增加土壤硝态氮含量,随着施氮时间的延长,氮磷添加显著增加土壤铵态氮。2)随着施氮时间的延长,氮添加和氮磷添加均能显著降低土壤pH值;磷添加对土壤pH值无显著影响。3)相对硝态氮含量的增加而言,相同程度的土壤铵态氮含量的增加后土壤pH值降低的幅度更大。
In order to understand the effects of N and P addition on soil available nitrogen and pH in a subtropical evergreen broadleaved forest dominated by Schima superba, we investigated contents of soil NH4^+-N, NO3^--N and pH. Four N and P addition treatments were included as follows: CK (no addition of N and P), N (50 kg N·hm^-2·a^-1), P (15 kg P·hm^-2·a^-1) and NP (100 kg N·hm^-2·a^-1+15 kg P·hm^-2·a^-1). The results showed that: 1) The soil NH4^+-N and NO3^--N concentrations were significantly increased after N addition, and the range of stimulation increased with prolonged nitrogen fertilization time. The soil NO3--N concentration was significantly decreased by P addition, and there was no significant impact on soil NH4+-N concentration under P addition. NP addition significantly increased the soil NO3^--N concentration, and N addition alone had more obvious effects on the soil NO3^--N concentration than NP addition. The response of soil NH4^+-N concentration to NP addition turned from insignificant to significant over time. 2) The soil pH decreased obviously with prolonged N addition and NP addition time, while remained stable under P addition. 3) Relative to the increase of nitrate nitrogen concentration, the same increase of soil ammonium nitrogen concentration resulted in a greater decline in pH value.